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<br />;; <br /> <br />11 <br /> <br />o <br />o <br />!:! <br /> <br />...... <br />...---- <br />./. <br />/' <br />../ <br /> <br />x <br />:3 <br />u.. <br />0:: <br />W <br />... <br /><( <br />3: <br />o <br />50 <br />Oei <br />:J'" <br />...J <br /><( <br />I- <br />o <br />I- <br />u.. <br />o <br />... <br />z <br />~ <br />0:: <br />W <br />a.. <br /> <br /> <br />o <br />ei <br /> <br />0.0 <br /> <br />10.0 20.0 <br />NUMBER OF 3-HOUR PERIODS <br /> <br />30.0 <br /> <br />40.0 <br /> <br />Figure ~ Cumulative frequency distribution showing the percen~ of liquid <br />water flux for 35 three ho~r periods durin~ the 1985 research season, 15 <br />January to 15 March. Values are ran~ed by percent. <br /> <br />-; <br /> <br />1 <br /> <br />-' <br /> <br />o <br />o <br />o <br />o <br />N <br /> <br />. <br /> <br />---. <br />"- <br />..c <br />,.., <br />~ <br />Q) <br />Q) <br />- <br /> <br />. <br /> <br />.. <br />. <br /> <br />Q) <br />\... <br />00 <br />o . <br />.......0 <br />o <br />XO <br />::>~ <br />...J <br />u.. <br />0:: <br />~ <br /><( <br />3: <br />o <br />5 <br />o <br />:J <br /> <br />. <br />. <br /> <br />. <br /> <br />. <br /> <br />.' <br /> <br />~' <br /> <br />... <br />. : <br /> <br />. <br /> <br />. <br /> <br />. <br />. <br />. . <br />. <br /> <br />. <br /> <br />. <br /> <br />'> <br /> <br />. <br /> <br />.. <br />.. . <br /> <br />o <br />o <br /> <br />. <br /> <br />, <br /> <br />-20.0 <br /> <br />-10.0 0.0 <br />700mb TEMPERATURE (C) <br /> <br />10.0 <br /> <br />Figure 3. Liquid w~ter flux for 35 three hour periods during 1986 research <br />season versus 700 mb temperature from Adamsvi lIe rawinsondes. <br />